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Research Highlights Topic: Air-Sea

Quantifying the contributions of surface forcing to sea level variability along the US Gulf Coast
Quantifying the contributions of surface forcing to sea level variability along the US Gulf Coast
Ocean eddies structure mean equatorial upwelling
Ocean eddies structure mean equatorial upwelling
What explains the interannual variability of O2 content and distribution in the tropical Pacific?
What explains the interannual variability of O2 content and distribution in the tropical Pacific?
Intrinsic biases in AGCM and OGCM
Tracing the origins of equatorial Pacific biases in a coupled climate model
Coupled air-sea simulations reveal the dynamics of surface wave growth and breaking-induced dissipation
Coupled air-sea simulations reveal the dynamics of surface wave growth and breaking-induced dissipation
How interfering waves drive the MJO
How interfering waves drive the MJO
The dynamics of the Atlantic extratropical–tropical teleconnections
The dynamics of the Atlantic extratropical–tropical teleconnections
Conversions between kinetic (Ek) and available potential (Ea) energy for upward-buoyant (ρ'<0) water parcels in the upper Tropical Pacific.
Beyond local wind: How remote forces shape Pacific equatorial upwelling
Figure from Villas Bôas, Marechal, and Bohé (2025)
Mapping the surface wave field in two dimensions: New insights from SWOT
Figure 1. The 35-year trends of winter-spring sea surface temperature, precipitation, and sea level pressure. a, observation of 1980-2014. Model-simulated 35-year trends for pre-industrial climate grouped and averaged for b, the strongest El Niño-like trends and c, the strongest  La Niña-like trends. Model-simulated 35-year trends for 1980-2014  grouped and averaged for the ensemble members d, with the strongest El Niño-like trends and e, with the strongest La Niña-like trends.
Drivers of the Southwestern US precipitation decline
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